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61.
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Sub-seasonal variability of Luzon Strait Transport in a high resolution global model 总被引:1,自引:1,他引:0
The Luzon Strait is the main impact pathway of the Kuroshio on the circulation in South China Sea (SCS). Based on the analysis of the 1997–2007 altimeter data and 2005–2006 output data from a high resolution global HYCOM model, the total Luzon Strait Transport (LST) has remarkable subseasonal oscillations with a typical period of 90 to 120 days, and an average value of 1.9 Sv into SCS. Further spectrum analysis shows that the temporal variability of the LST at different depth is remarkable different. In the upper layer (0–300 m), westward inflow has significant seasonal and subseasonal variability. In the bottom layer (below 1 200 m), eastward outflow exhibits remarkable seasonal variability, while subseasonal variability is also clear. In the intermediate layer, the westward inflow is slightly bigger than the eastward outflow, and both of them have obvious seasonal and subseasonal variability. Because the seasonal variation of westward inflow and eastward outflow is opposite, the total transport of intermediate layer exhibits significant 50–150 days variation, without obvious seasonal signals. The westward Rossby waves with a period of 90 to 120 days in the Western Pacific have very clear correlationship with the Luzon Strait Transport, this indicates that the interaction between these westward Rossby waves and Kuroshio might be the possible mechanism of the subseasonal variation of the LST. 相似文献
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There exists a tongueshaped swelldominance pool known as Swell Pool (SP) in the Eastern Pacific region. The monthlymean wave transports (WT) for each month of 2000 is computed using the wave products of ECMWF reanalysis data. By comparing the 2000 monthlymean WT and monthlymean wind field from QUICKSCAT, large differences are found between the wave transport direction and the wind direction over the Eastern Pacific. This may serve as an evidence for the existence of the SP in this region. The work done in this study indicates that the sources of swell in the Tropical Eastern Pacific (TEP) are in the westerly regions of the Southern and Northern Pacific. 相似文献
65.
A dual channel difference (DCD) method is applied to detect nighttime sea fog/stratus over the Huanghai Sea using the infrared (IR) data of shortwave (3.5–4.0 μm) and longwave (10.3–11.3 μm) channels from the Multi-functional Transport Satellite (MTSAT)-1R, i.e., shortwave minus longwave brightness temperature difference (SLTD). Twenty-four sea fog events over the Huanghai Sea during March to July of 2006 and 2007 are chosen to determine a suitable value of SLTD for nighttime sea fog/stratus detection, and ... 相似文献
66.
The results of the new concept of coastal sea circulation are demonstrated by numerical simulations for the first time. The numerical experiments in three types of rectangular model seas illustrate the dependence of circulation on tidal phases due to the convectively nonlinear effect which is estimated by a newly defined drift dispersion in-dex. Then, the present theory is applied in the Bohai Sea of China. At the Bohai Straits and the Huanghe River mouth area the circulation direction even reverses owing to different initial tidal phases which shows that the the-ory copes with nonlinearity well. The calculated M2 tide-induced residual circulation shows that a clockwise gyre exists in the center of an anticlockwise gyre in the central Bohai Sea due to the topographic features. In the Bo-hai Gulf the tide induced circulation shows a 3D structure with outflow at the surface and the inflow at the bottom which can partly explains the spread of the Huanghe River fresh water out of the Bohai Gulf and the inflow of the sediment from the Huanghe River. 相似文献
67.
深海经济问题国际研究动态及启示 总被引:1,自引:0,他引:1
深海经济问题已经成为国际学术界关于海洋经济问题研究的新领域.文章从深海资源与环境、深海渔业、深海工业和深海运输等方面对深海经济国际文献进行了初步梳理,以期为我国深海经济问题的深入研究提供借鉴. 相似文献
68.
A Lagrangian tracer model is set up for Hangzhou Bay based on Coupled Hydrodynamical Ecological model for Regional Shelf Sea
(COHERENS). The study area is divided into eight subdomains to identify the dominant physical processes, and the studied periods
are March (the dry season) and July (the wet season). The model performance has been first verified by sea-surface elevation
and tidal current observations at several stations. Eight tracer experiments are designed and Lagrangian particle tracking
is simulated to examine the impact of physical processes (tide, wind and river runoff) on the transport of passive tracer
released within the surface layer. Numerical simulations and analysis indicate that: (1) wind does not change the tracer distribution
after 30 days except for those released from the south area of the bay during the wet season; (2) the tide and the Qiantang
River runoff are important for particle transport in the head area of the bay; (3) the Changjiang River runoff affects the
tracer transport at the mouth of the bay, and its impact is smaller in the dry season than in the wet season.
Supported by the Natural Science Foundation of China (No.40576080); National High Technology Research and Development Program
of China (863 Program, No. 2007AA12Z182) 相似文献
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